When the base of a glacier melts and refreezes, it creates a layer of water that can facilitate movement, allowing the glacier to slide over the bedrock more easily. This process can lead to the formation of features like subglacial lakes and can affect the glacier's overall dynamics and stability. Additionally, the melting and refreezing can alter the glacier's internal structure, potentially influencing its flow patterns and contributing to its eventual retreat.
Heat does not affect it. It expands with coolness. It contracts with heat.
Changing the temperature can affect the fluidity and movement of molecules within the chloroplast membranes. Extreme temperatures can denature proteins involved in chloroplast movement, leading to impaired function and reduced movement. Additionally, temperature changes can affect enzyme activity within the chloroplasts, influencing their overall metabolic processes and movement.
The shape of a glacier is primarily determined by the interplay of gravity, the underlying topography, and the accumulation and melting of ice and snow. Glaciers flow downhill due to gravity, adapting their form to the landscape they traverse, which can include valleys, ridges, and other geological features. Additionally, variations in temperature and precipitation affect the glacier's mass balance, influencing its thickness and extent. As a result, the combination of these factors creates diverse glacier shapes, from broad, slow-moving ice sheets to steep, narrow valley glaciers.
A lesion in the cerebral peduncles can affect motor function, resulting in symptoms such as weakness, clumsiness, or difficulty with coordination. It can also lead to changes in eye movement and altered consciousness levels.
A glacial tilt refers to the angle at which a glacier is tilting or inclining. This tilt can affect the movement and stability of the glacier, impacting its flow and potential for calving.
Basal drag force is the resistance on a glacier's base as it moves over its bed. It occurs due to the friction between the glacier and the underlying rock or sediment. The amount of basal drag force can affect the speed and movement of the glacier.
The glacial movement was caused the formation of fjords, created Norway's jagged coastline and, removed soil, making the land rocky: answer by RAID 1er; Improved by kodiak13 Now that i have answered your question can i please have a hambuger some chicken and a hotdog can you make that an extra large if you don't mind
Throughout history Denmark's location has made it a link for people and goods between the Nordic countries and Europe.
When the base of a glacier melts and refreezes, it creates a layer of water that can facilitate movement, allowing the glacier to slide over the bedrock more easily. This process can lead to the formation of features like subglacial lakes and can affect the glacier's overall dynamics and stability. Additionally, the melting and refreezing can alter the glacier's internal structure, potentially influencing its flow patterns and contributing to its eventual retreat.
like others in other countries nearby. the same approach and action
wind, water, waves, & glacier
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it encouraged other countries to speak out in favor of colonialism.
Melt water
Does the Quran affect the laws and countries
It diverted the attention of the colonizer countries, which gave the colonized people a chance to revolt and fight for their independence.